Business Financing and the Capital Structure Assignment

Business Financing and the Capital Structure - Assignment Example The total cost of each resource has to be determined and summarized. On the basis of the summarized reports of cost of resources, a budget will be prepared by the finance and accounts department which would help the organization to determine next course of action (Summers, 2011, pp.2-11). Working Capital Management Proper working capital management is necessary to carry out day to day business operations. It is defined as the difference between current assets and liabilities. Thus, the objective of working capital management is to maintain a balance between current assets and liabilities. Positive difference or surplus funds can be used to make planned expenses such as payment of short term obligations and salaries. The working capital is negative or deficit when the current liabilities exceed current assets that would require the firms to borrow short term funds in order to manage the deficit (Ganesan, 2007, pp.1-2). When the working capital is positive, the firm would have surplus short term funds which can be invested in the money market instruments. The maturity of money market instruments are less than one year and hence investment in money market is less risky. This is because, the status of any business can be more or less accurately predicted in short term whereas the same becomes uncertain as the maturity increases due to increased chances of borrower to default. Some important money market financial instruments are discussed as follows: Commercial papers (CP) – They are issues by highly rated corporate entities and classified as short term unsecured promissory notes issued at discount and redeemed at face value. Certificate of Deposit (CD) – It is similar to ordinary time deposit differing only in maturity period and interest rates. They are issued by banks and the interest rates are generally higher than savings deposit rates. Municipal notes – Short term financial security issued by municipality in expectation of tax receipts as revenues. Treasury bills – They are debt instruments issued by the government whose maturity ranges from 3 to 12 months. Repurchase agreements – they are short term loans that are arranged by an investor to whom securities would be sold with an agreement to repurchase them back on a future date at pre-determined fixed rate. Thus, a corporate organization may park their excess generated from efficient working capital management in above discussed financial instruments that are liquid and used as marketable securities. Financial Instruments of Securities Market Every organization invests capital in business to finance its operations and generates goods and services to meet demands and earn profit. As the business expands its operations more funds are required to carry out business objectives. The financial sources may be broadly classified into equity and debt. Funds can be raised from these sources in the financial securities market. The securities market may be furthe r divided into primary or secondary securities market. In the primary securities market only those securities are issued that are participating in securities market for first time and the process is known as IPO (Initial Public offering). The secondary market is a place for traders who buy or sell differ securities.

Managing Activities to Achieve Results Essay Example | Topics and Well Written Essays - 3000 words - 2

Managing Activities to Achieve Results - Essay Example Tesco’s website states that the vision of the company is â€Å"for Tesco to be most highly valued by the customers we serve, the communities in which we operate, our loyal and committed staff and our shareholders; to be a growth company; a modern and innovative company and winning locally, applying our skills globally† (Tesco Plc, 2011b). This can be broken down into four key aspects each of which has implications for the structure and culture of the business.-  To be the most highly valued business: to be highly valued as a business, Tesco needs to continue its focus on satisfying customers. This involves all levels of management. Specifically, the company needs to ensure that the customers are happy with the service they receive at the individual level, through interactions with frontline (level one) staff. In addition, value within the company image must be maintained, with business advertising and actions reflecting their desire to help the customer. This can be s een in the focus of the company culture on satisfying customers, and in the manner in which all levels of the business interact and communicate with one another. -  To remain a growth company: the organisational structure of Tesco allows for significant communication across different areas of the business. Because of this, the company is able to quickly adapt to any important events such as sudden demand for a particular item or a national or global crisis.The company visualizes itself to be serving and retaining its loyal customers.... Tesco Plc’s company culture is to consider that their customers are above all else and aim to give customers a positive experience to ensure that they continue to shop at the company . To achieve this all the levels of management within the organisation interact and communicate efficiently with one another with a strong focus on customer service and customer satisfaction. 1b) Tesco’s website states that the vision of the company is â€Å"for Tesco to be most highly valued by the customers we serve, the communities in which we operate, our loyal and committed staff and our shareholders; to be a growth company; a modern and innovative company and winning locally, applying our skills globally† . This can be broken down into four key aspects each of which has implications for the structure and culture of the business. To be the most highly valued business: to be highly valued as a business, Tesco needs to continue its focus on satisfying customers. This involves all levels of management. Specifically, the company needs to ensure that the customers are happy with the service they receive at the individual level, through interactions with frontline (level one) staff. In addition, value within the company image must be maintained, with business advertising and actions reflecting their desire to help the customer. This can be seen in the focus of the company culture on satisfying customers, and in the manner in which all levels of the business interact and communicate with one another. To remain a growth company: the organisational structure of Tesco allows for significant communication across different areas of the business. Because of this, the company is able to quickly adapt to any important events such as sudden demand for a particular item or

Fire Protection Hydraulics and water supply Essay - 1

Fire Protection Hydraulics and water supply - Essay Example According to Edwards (2004), firefighting is an act which involves putting off destructive fires with the assistance of firefighters. Firefighting as a profession requires immense training and education for several years. A firefighter is required to demonstrate good communication skills, good judgment, mechanical aptitude, basic math skill among others. Basic mathematics has become one of the vital requirements among the fire fighters due to the various activities they carry out. For instance, fire fighters require the basic knowledge of calculating the amount of water required to suppress a fire in a closed volume. Therefore, basic mathematics plays a critical role in assisting the firefighter to decide on the amount of water required to extinguish the fire. Field fire workers and engineers are the common positions which require basic mathematics on a regular base (Edwards, 2004). Their main roles of the firefighters include: disaster management, search and rescue, fire prevention, emergency medical service and hazardous material response. However, fire fighting is a dangerous and complex act. Hence an increase need for basic mathematics.

Recruitment At Richer Sounds Essay Example for Free

Recruitment At Richer Sounds Essay John Clayton is the training and recruitment director within the business. His two key areas are the colleague support or the recruitment/training office. He works closely with the manager of colleague support, Tracey Armstrong. Richer Sounds personal views on Recruitment Richer Sounds always tries to recruit people who have friendly personalities and like to enjoy their work. The company looks for these keys on candidates rather than much of their grades because normally these people normally start to work as a sales person or work in the support department. The promotion policy in Richer Sounds enables efficiently working colleagues to be promoted up in the company rather than recruiting new employees who have no understanding within the business. Richer Sounds only recruit employees if they need someone who has the skills to do particular work such as professional in I.T. How Richer Sounds advertise for new colleagues Within every edition of the in-store catalogue and website they advertise their vacancies, these vacancies are usually for needs of new sales person or need new employees to work in the departments. This generates ongoing application from many interested people. If there are no vacancies at that time then they keep all record of people who applied, for about six months. Colleagues are also able to advice his/hers friends o relatives to work in the company, however these applicants should also follow the same rule of application as all other people. These adverts causes the company to save major amount of money each time because if they would publish it on the newspaper everytime then they would have to pay certain amount to the newspaper company therefore this idea of having to publish on their catalogues and website is good idea. If the company doesnt receive any phone call from any people regarding the job then finally the company will have to publish it on the newspapers. For specialist employees to recruit the company notifies the vacancy to the employment agency. The recruitment process at richer sounds The recruitment process is shown on the following steps: Identify any vacancies within the business Advertise the vacancies The company the looks through all the CVs relevant to that store or department They schedule for interviews with appropriate store or department manager. In Richer Sound all managers have completed their Managers Development Course and while doing they also received training on interview, how to interview a candidate. The applicant which is been successful is been given a trial day to work at richer sounds If all the interview and trial day is completed and the candidates are successful then the candidates can either send an application form which states that he/she is agreeing to work with richer sounds. Next all these new candidates have to meet either Jez Avens, John Clayton or Lee Nelson for their final approval When the company receives the application form, the business then sends these forms for references and as the candidate gets one or more good reference he/she is offered the job. They then write a letter to the candidate, which also includes the statement of terms of employment. Final step for the company is to send off letters to all candidates given an interview regarding that they have given this job to someone. This is given so the candidates would know if he/she would get the job. The company policy and rules Richer sounds have several policies on recruitment so they do not operate within the law but also operate truthfully. These include The companys equal opportunities statement. The test shouldnt require high level of English Richer Sounds never ask a woman about their family

Canadian forests Essay Example for Free

Canadian forests Essay Gary Paulson’s Hatchet is set in Hampton, New York, but mainly in the north Canadian forests, in particular a region known as the Canadian Shield. The main characters of the novel are Brian Robeson, the protagonist, a thirteen year old boy; his parents; and two pilots, one of whom flies Brian into north Canada before giving up the ghost at the controls, and the second pilot who rescues the young boy stranded in the wilderness. The main events of the novel revolve around Brian, who travels by airplane, Cessna 406, from his hometown, Hampton, New York, to visit his father who is working as a mechanical engineer in a Canadian oil field. The young boy’s parents are divorced, and this is the first summer that Brian is going to spend with his father after the divorce. Brian travels as a single passenger in the airplane, before the pilot of the plane dies of a heart attack leaving the young boy to crash land the airplane all by himself. The plane lands in an isolated lake somewhere in the north Canadian forests. And, Brian possesses nothing to face the tragedy, except a hatchet that his mother had presented to him before his departure. The hatchet thus becomes the boy’s tool for survival in the wilderness. He must figure out how to make fire by striking the hatchet’s blade against a rock. He must also figure out what to eat in order to survive. Moreover, he must deal with unusual circumstances such as the presence of a bear, a porcupine, a moose, a skunk, in addition to a tornado. Eventually, the boy learns to hunt and fish after making special tools for himself. The events proving Brian’s ability to manage himself in the wilderness are very important in the novel. The last major event occurs after a violent storm that hits the forest and tosses the wreckage of the airplane to the land surface. The teenager manages to break into the airplane to recover the survival pack. He finds a transmitter in the pack, which, upon activation, connects him to a pilot who finally comes to rescue him in an airplane. The main conflict in the novel is between Brian, the protagonist, and nature, the antagonist. The young boy must find a way to overcome the unusual circumstances he finds himself in. He must struggle against threats posed by wild animals as well as natural disasters. Similarly, he must fight against his own natural tendency to give up in the face of the difficulties that confront him. Another conflict presented in Hatchet is between Brian’s natural, emotional weakness and the strength that he needs to gain emotional freedom. The boy knows a Secret about his mother that had led to his parents’ divorce. Time and again the Secret confronts him with emotional distress. Yet, Brian must learn to let go of the distress and face the challenge of accepting his circumstances as they are. The novel thus deals with maturity – the theme of growing up from boyhood to manhood. Brian has no human being to rely on at the time that he is stranded in the wilderness. Yet, he must face all sorts of dangers to find his way out of his troubles, both emotional and physical. The major strength of the novel is that Brian succeeds despite all odds, using his intelligence as best as possible. He finds his way out. Hence, his story becomes a lesson for all teenagers who may or may not face the kinds of challenges that Brian faces. The story is also recommended for young readers of fifth and sixth grades, who are sure to be inspired by Brian’s spirit of strength and endurance. As a matter of fact, even adults may be able to remind themselves about the resilient, surviving spirit of humanity by reading Hatchet. Thus, the novel may be recommended for all readers.

Overview of the Grace-Fo Satellite Mission

Overview of the Grace-Fo Satellite Mission The Gravity Recovery and Climate Experiment Follow-On: An Overview An artist depiction of the GRACE satellite configuration (Sharing, 2017) The field of remote sensing is continuously expanding and adapting to yield new information about the earth and its complex systems. Modern satellite technology has expanded to be able to monitor spatial and temporal variations in Earths global gravity field (Schutze, 2016). The ability to monitor the Earths geoid now allows scientists to understand changes in hydrological characteristics on the surface of the planet including ice mass loss due to climate change and sea level rise (NASA JPL, 2017). The Gravity Recovery and Climate Experiment (GRACE) and its follow-on mission represent the application of this new technology that is essential for obtaining new data about global mass redistribution. The GRACE-FO mission will offer benefits due its use of active sensors and new technological inputs, but with any satellite system, there will be sources of error and challenges in design and data usage. The first GRACE mission was launched in 2002 as a result of the combined efforts of the US National Aeronautics and Space Administration (NASA) and the Helmholtz Centre Potsdam German Research Centre for Geosciences (GFZ) with assistance from partner institutions of both leading agencies (Schutze, 2016). The primary goal of the mission was to provide a new model of Earths gravity field every 30 days (Schlepp et al., 2015). Two identical satellites comprise the system with one trailing behind the other by 220km in a sun-synchronous orbit (Wahr, 2007). The satellites fly in a low polar orbit of 450 km and, the system circles the Earth every 90 minutes (Schutze, 2015). Spatial variations in Earths gravity field lead to different accelerations in the two satellites and therefore, differing inter-satellite separation (Schutze, 2016). Therefore, the GRACE mission is different than many other earth observation satellite missions because it does not make measurements of electromagnetic ener gy reflected back to it from Earths surface. The distance between the two satellites serves as the source of data. Also, uniquely, the satellites are left mostly without intervention to their orbit unless they separate by less than 170 km and more than 250 km (Sheard et al., 2012). Illustration of the positions of the two GRACE satellites in response to variations in Earths gravity field; a)The two satellites pass over the ocean and neither is affected; b)The lead spacecraft encounters a change in gravity over the more dense land mass and pulls away from the trailing spacecraft; c)The lead spacecraft moves back over water but now the trailing spacecraft changes position in response to the greater pull of gravity over the land mass (Ward, 2003) The first GRACE mission was only planned to run for 5 years, but far exceeded this as it is now in its 15th year of operation. The batteries in each satellite are fatiguing and accurate data is increasingly available in more irregular intervals (Gà ¶rth et al., 2016). As a result, NASA and the GFZ created a follow-on mission to prevent data gaps (Schlepp et al., 2015). The follow-on was approved for launch in August 2017 and is known simply as the Gravity Recovery and Climate Experiment Follow-On (GRACE-FO) mission (Schlepp et al., 2015). The primary objective for this mission is the same as the previous; to create monthly global gravity models for five years (Sharing Earth Observation Resources, 2017). The GRACE-FO mission will use some of the key sensor technology and overall design of the first GRACE mission, but will also include unique features. The same two-satellite design will remain but the inter-satellite distance will be reduced from 220 km to 50 km (Zheng and Xu, 2015).   Several very important pieces of equipment will carry over from the first mission to each of the GRACE-FO satellites but will see improvements in design. This includes a microwave instrument (MWI) dependent on Global Positioning System (GPS) technology. The MWI system measures the distance between the satellites centers of mass and slight changes in distance represent gravitational changes (Tapley, 2008). A very sensitive accelerometer meant to measure the forces acting on the satellites besides gravity including atmospheric drag will also remain (Tapley, 2008). There were previous accelerometer errors and satellite-to-satellite measurement errors that will be reduced by the lower altitude and up dates in design on the follow-on mission (Loomis, Nerem, and Luthcke, 2012). The microwave ranging system employed can measure the distance between satellites to within one micron or about the diameter of one human blood cell (NASA JPL, 2017). It is known as a KBR system because it utilizes microwaves in the K (26 GHz) and Ka (32 GHz) frequency channels (Jiang et al., 2014). Distance measurements between the two satellites are taken by monitoring the time of flight of microwave signals transmitted and received nearly simultaneously between the two spacecraft (Bao et al., 2005). Previously collected data and models created by scientists based on known gravitational differences linked to mountains and ocean trenches, the location of the sun, and the flow of the tides are compared to new measurements of the satellites to interpret gravitational changes (NASA JPL, 2017).   Also, the GPS unit on board is used in tandem with the MWI to be able to understand the gravity field below and can accurately assign capture time to data (Sheard et al., 2012). The accelerometer can then measure non-gravitational forces affecting the satellite as previously mentioned including atmospheric drag and solar radiation pressure (Schutze, 2016). These additional forces are then subtracted from measurements taken by the MWI. At the low altitude of orbit of GRACE comes changing solar radiation and large thermal disturbances to on-board instruments (Schutze, 2016). As a result, one improvement to the accelerometer on the GRACE-FO satellites will be placing the measurement digitalization unit in a temperature controlled area of the spacecraft to prevent temperature variation that can make data inaccurate (Christophe et al., 2015). The FO mission will include new technology known as a laser interferometer that will make measures that are at least 25 times more precise than the on-board microwave ranging system due to shorter wavelength usage (Sharingà ¢Ã¢â€š ¬Ã‚ ¦, 2017). The LRI uses an active transponder principle, which means that the weak incoming received (RX) beam to the trailing satellite is replaced by a strong local oscillator (LO) beam. The LO beam is then reflected back to the lead satellite by a Triple Mirror Assembly (TMA) which directs the beam and influences the amount of light returned (Fledderman et al., 2014). It also serves to effectively route the incoming beam around other important hardware pieces (Fledderman et al., 2014). The use of the new laser interferometer represents the first time an active laser ranging system will be operated between two spacecraft (NASA JPL, 2017). However, the microwave system will remain intact to ensure continuity of data from the first mission and the use of interferometer represents only a technology demonstration (Sharingà ¢Ã¢â€š ¬Ã‚ ¦, 2017). While some studies found the LRI technology could greatly increase the accuracy of gravity data, others found that there would be only moderate improvements in the accuracy models (Flechtner et al., 2015). However, seeing the results of the two systems as they operate simultaneously will create meaningful data for the planning of future of gravity field missions. The GRACE-1 mission allowed for new breakthroughs in the fields of hydrology, oceanography, glaciology, geophysics, and geodesy (Sharingà ¢Ã¢â€š ¬Ã‚ ¦, 2017). Since gravity is determined by mass, the GRACE systems have the capability to show how mass is distributed around the planet (Sharingà ¢Ã¢â€š ¬Ã‚ ¦, 2017). However, GRACE has and will continue to have no vertical resolution and can therefore, not distinguish between surface water, soil moisture, and ground water (Bolton and Thomas, 2015). Land surface models therefore allow for the disaggregation of Terrestrial Water Storage (TWS) data by separating these data into layers with known points of distinction (Bolton and Thomas, 2015). For example, in a study of the High Plains region of the US, the variability of snow and surface water were found to make insignificant contributions to TWS variability compared to groundwater and soil moisture changes (Ward, 2003). Therefore, removing moisture data known from previous studies of th e region allowed scientists to subtract these figures from the GRACE gravitational measurements to understand changes in groundwater levels over time (Ward, 2003). Over time, improvements in GRACE data processing have allowed for the detection of changes in TWS within 1.5 cm accuracies for a wide range of spatial and seasonal scales (Jiang et al., 2014). (Ward, 2003) Measuring changes in global mass distribution can help scientists across many disciplines. GRACE data has also been used to observe increases and decreases in the ice and snow masses of glaciers and changes to the solid Earth following seismic activity such as the Fukushima earthquake of 2011 in Japan (Flechtner et al., 2016). Ocean water elevation changes caused by the devastating 2004 Sumatra tsunami had an impact of the inter-satellite distance of the GRACE satellites and showed how oceanic mass redistribution can affect Earths gravity field (Bao et al., 2005). Due to the relatively low spatial resolution of GRACE data, it is more useful for monitoring large-scale terrestrial water changes such as in past studies of the entire Amazon Basin or India (Bolton and Thomas, 2015). Other applications include flood and drought monitoring for management projects and interventions (Bolton and Thomas, 2015).   For example, the US National Drought Mitigation Center uses GRACE data mont hly to generate drought indicators and monitor surface water changes (NASA JPL, 2016). GRACE data also allows for the study of changes in deep ocean currents by measuring pressure changes at great depths. Similar pressure changes in the structure of the solid earth can be studied as well (NASA JPL, 2016). Trends in TWS and water mass redistribution made possible from GRACE data from 2002-2013 (Bolton and Thomas, 2015) One of the benefits of an active satellite system such as the GRACE-1 and GRACE-FO compared to passive systems is that it can collect accurate data 24 hours per day because it creates its own source of electromagnetic energy (Schowengerdt, 2006). Also, the use of microwaves in the GRACE missions means that data is not affected by any type of cloud cover which often greatly affects accurate passive sensor data acquisition because the system only considers inter-satellite distance and GPS location for data retrieval. Active sensors dependent on microwave signals like on the GRACE missions are unique in their capabilities. The launch of the first GRACE mission allowed for data on earths geoid that was 100 to 1000 times more accurate than previous models could estimate depending on the region of the global under consideration (Ward, 2003). GRACE data has also allowed scientists to under the impact of global climate change based on mass redistribution of water around the globe in a comprehensive and consistent manner never previously achieved. With more accurate data from the GRACE-FO mission and the security of continued data creation, changes caused by climate change will continue to be monitored and planning for issues such as drought can be improved. However, compared to passive system data, the analysis of data is more complex and costly overall. The data output of the GRACE systems also requires a lot of manipulation and filtering to create meaningful datasets for a variety of disciplines. The microwave region of the electromagnetic spectrum is far from the visible region and therefore, the resulting data is also less intuitive for human interpretation (Schowengerdt, 2006). The raw data outputs for GRACE are just inter-satellite distance measurements and GPS data about satellite location (Ward, 2003). Therefore, improvements in satellite technology components alone will not improve the data created by GRACE. Improvements also need to be made to the many geophysical models used in data processing (Loomis, Nerem, and Luthcke, 2012). For example, a complete global depiction of the earths gravity field is only available every 30 days while forces such as tidal shifts can change on a minute-to-minute basis. This difference creates an issue in which short-term differences are lost or their impact is underestimated (Sheard et al., 2012). Therefore, understanding gravitational influences not directly linked to mass balance changes is essential. Models of gravity field anomalies on earths geoid created by comparing GRACE data from two different temporal scales (Ward, 2003) Models based on GRACE data are also limited by the noise present in the system data. This noise is linked to instrument errors, uncertainties in background models, and limitations in processing strategies (Siemes et al., 2013). In order to make meaningful measurements of mass changes on the earth using GRACE data, the noise of resulting models needs to be kept at a minimum, usually accomplished by applying filters (Siemes et al., 2013). However, when one problem is solved, another potentially arises. Filtering suppresses noise and blurs the signal, limiting the spatial resolution so much that part of the leak may affect nearby regions and cause errors in mass redistribution data (Siemes et al, 2013). However, more complex filtering methods have been developed to also minimize the blurring of data. Also, the spatial resolution of GRACE data is ultimately limited (Siemes et al., 2013). The spatial range for very accurate GRACE data application was 400km to 40,000 km for the first mission (Tapley, 2008). The strength of GRACE data therefore lies in an ability to monitor mass changes over time rather than to understand the water storage in one area at a specific time. However, there is potential for the lower altitude of the GRACE-FO mission and the LRI technology utilization of shorter wavelengths to allow for higher spatial resolution. The GRACE mission have shown that the use of active sensor technology on earth system satellite missions that utilizes microwave laser instruments and likely laser interferometers is incredibly efficient at understanding changes in earths geoid. With the launch of the GRACE-FO mission later this year, even more accurate measurements and greater understanding of mass redistribution of water around the planet will be possible. Despite the rapidly changing and unpredictable political climate of the United States government, the launch of the GRACE-FO mission seems undeterred and the collection of important data related to climate change-related issues will continue to be gathered. References Bao, L.F., Piatanesi, A., Lu, Y., Hsu, H.T., and Zhou, X.H. (2005) Sumatra tsunami affects observations by GRACE satellites. Eos, Transactions American Geophysical Union, 86(39), 353-356. Bolton, J. and Thomas, B. (2015) Overview of the Gravity Recovery and Climate Experiment (GRACE) data and applications. NASA Applied Remote Sensing Training (ARSET). Powerpoint Presentation. http://www.cazalac.org/mwar_lac/fileadmin/imagenes2/Remote_Sensing/S5P1.pdf [2.3.17]. Christophe, Boulanger, Foulon, Huynh, Lebat, Liorzou, and Perrot. (2015) A new generation of ultra-sensitive electrostatic accelerometers for GRACE Follow-on and towards the next generation gravity missions. Acta Astronautica, 117, 1-7. Flechtner, F., Neumayer, K., Dahle, C., Dobslaw, H., Fagiolini, E., Raimondo, J., and Gà ¼ntner, A. (2016) What can be expected from the GRACE-FO laser ranging interferometer for earth science applications? Surveys in Geophysics, 37(2), 453-470. doi:10.1007/s10712-015-9338-y. Fleddermann, Ward, Elliot, Wuchenich, Gilles, Herding, . . . Shaddock. (2014) Testing the GRACE follow-on triple mirror assembly. Classical and Quantum Gravity, 31(19), 12. Gà ¶rth, A., Sanjuan, J., Gohlke, M., Rasch, S., Abich, K., Braxmaier, C., and Heinzel, G. (2016) Test environments for the GRACE follow-on laser ranging interferometer. Journal of Physics: Conference Series, 716(1), 4. Jiang, D., Huang, Y., Fu, J., Wang, J., Ding, X., and Zhou, K. (2014) The review of GRACE data applications in terrestrial hydrology monitoring. Advances in Meteorology, 2014, Vol.2014. Loomis, Bryant D., Nerem, R. S., and Luthcke, S. B. (2012) Simulation study of a follow-on gravity mission to GRACE.(Report). Journal of Geodesy, 86(5), 319. NASA Jet Propulsion Laboratory (JPL). (2016). Applications overview. NASA. GRACE Tellus: Gravity Recovery and Climate Experiment. https://grace.jpl.nasa.gov/applications/overview/ [2.3.17]. . (2017) GRACE-FO. NASA. GRACE Tellus: Gravity Recovery Climate Experiment. https://grace.jpl.nasa.gov/mission/grace-fo/ [2.3.17]. Schlepp B., Kirschner M., Sweetser T.H., Klipstein W.M., Dubovitsky S., (2015). Flight Dynamics Challenges for the GRACE Follow-On Mission. 25th International Symposium on Space Flight Dynamics (ISSFD). http://elib.dlr.de/98835/1/ISSFD2015_FD%20Challenges%20for-20GRACE-FO_Schlepp.pdf [2.3.17]. Schowengerdt, R. (2006) Remote Sensing [electronic resource] : Models and Methods for Image Processing (3rd ed.). Burlington: Elsevier Science, 204-243. Schà ¼tze, D. (2016) Measuring Earth: Current status of the GRACE Follow-On Laser Ranging Interferometer. Journal of Physics: Conference Series, 716(1), 6. . (2015) LISA technology sheds light on climate change: GRACE-FO mission. LISA Mission. Youtube. https://www.youtube.com/watch?v=tb29hD3OgFw [2.3.17]. Sharing Earth Observation Resources. (2017) GRACE-FO (Gravity Recovery and Climate Experiment Follow-On)/ GFO (GRACE Follow-On). EO Portal Directory. https://directory.eoportal.org/web/eoportal/satellite-missions/g/grace-fo [2.3.17]. Sheard, B., Heinzel, S., Danzmann, G., Shaddock, K., Klipstein, D., and Folkner, A. (2012) Intersatellite laser ranging instrument for the GRACE follow-on mission. Journal of Geodesy, 86(12), 1083-1095. Siemes, C., Ditmar, P., Riva, R., Slobbe, E., Liu, M., and Farahani, D. (2013) Estimation of mass change trends in the Earths system on the basis of GRACE satellite data, with application to Greenland. Journal of Geodesy, 87(1), 69-87. Tapley, B. (2008) Gravity model determination from the GRACE mission. The Journal of the Astronautical Sciences, 56(3), 273-285. Wahr, J. (2007) Time Variable Gravity from Satellites-3.08. In Treatise on Geophysics, 218. Ward, A. (2003) Weighing earths water from space: challenges and limitations to using the GRACE technique. NASA Earth observatory. http://earthobservatory.nasa.gov/Features/WeighingWater/printall.php [7.3.17]. Zheng Wei and Xu Houze. (2015) Progress in satellite gravity recovery from implemented CHAMP, GRACE and GOCE and future GRACE follow-on missions. Geodesy and Geodynamics, 6(4), 241-247. doi:10.1016/j.geog.2015.05.005

Big Mamas Funeral :: Mama Funeral

Big Mama's Funeral Gabriel García Márquez story, Big Mama's Funeral, is a story filled with fantastical scenes and events much in line with Don Quixote and Candide. The introductory paragraphs of Big Mama's Funeral and Candide sound so similar in voice the two authors could be mistaken for the same. In Candide, one finds a series of episodes that are so far from the truth and yet perfectly explainable. The story of the fate of Dr. Pangloss, the death and resurrection of Cunegund and of her Jesuit brother, and the story of the old woman with one buttock are farcical in the same way as the episodes in Big Mama's Funeral. In Don Quixote, we find a man, for the most part average, who wishes to become a knight-errant. In his quest is as series of happenings so ridiculous they are nothing short of tabloid-style sensationalism, or drug induced hallucinations. In Big Mama's Funeral, we are told the story of the death and funeral of Big Mama. In the events of her life and the days proceeding and proceeding her death we find events and stories of the past that are truly fantastical. In the annals of her past we find that in her family the "uncles married the daughters of their nieces, and the cousins married their aunts, and the brothers their sisters-in-law, until an intricate mesh of consanguinity was formed." Here, García Márquez takes the simple act of incestuous relationships, which do occur, and elevates them to an extreme level. This is the writing style of García Márquez and the two aforementioned writers, Cervantes and Voltaire. Big Mama's Funeral :: Mama Funeral Big Mama's Funeral Gabriel García Márquez story, Big Mama's Funeral, is a story filled with fantastical scenes and events much in line with Don Quixote and Candide. The introductory paragraphs of Big Mama's Funeral and Candide sound so similar in voice the two authors could be mistaken for the same. In Candide, one finds a series of episodes that are so far from the truth and yet perfectly explainable. The story of the fate of Dr. Pangloss, the death and resurrection of Cunegund and of her Jesuit brother, and the story of the old woman with one buttock are farcical in the same way as the episodes in Big Mama's Funeral. In Don Quixote, we find a man, for the most part average, who wishes to become a knight-errant. In his quest is as series of happenings so ridiculous they are nothing short of tabloid-style sensationalism, or drug induced hallucinations. In Big Mama's Funeral, we are told the story of the death and funeral of Big Mama. In the events of her life and the days proceeding and proceeding her death we find events and stories of the past that are truly fantastical. In the annals of her past we find that in her family the "uncles married the daughters of their nieces, and the cousins married their aunts, and the brothers their sisters-in-law, until an intricate mesh of consanguinity was formed." Here, García Márquez takes the simple act of incestuous relationships, which do occur, and elevates them to an extreme level. This is the writing style of García Márquez and the two aforementioned writers, Cervantes and Voltaire.